Scaling of natural convection of an inclined flat plate: ramp cooling condition
Saha, Suvash C., Patterson, John C., and Lei, Chengwang (2010) Scaling of natural convection of an inclined flat plate: ramp cooling condition. International Journal of Heat and Mass Transfer, 53 (23-24). pp. 5156-5166.
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A scaling analysis is performed for the transient boundary layer established adjacent to an inclined flat plate following a ramp cooling boundary condition. The imposed wall temperature decreases linearly up to a specific value over a specific time. It is revealed that if the ramp time is sufficiently large then the boundary layer reaches quasi-steady mode before the growth of the temperature is finished. However, if the ramp time is shorter then the steady state of the boundary layer may be reached after the growth of the temperature is completed. In this case, the ultimate steady state is the same as if the start up had been instantaneous. Note that the cold boundary layer adjacent to the plate is potentially unstable to Rayleigh–Bénard instability if the Rayleigh number exceeds a certain critical value for this cooling case. The onset of instability may set in at different stages of the boundary layer development. A proper identification of the time when the instability may set in is discussed. A numerical verification of the time for the onset of instability is presented in this study. Different flow regimes based on the stability of the boundary layer have also been discussed with numerical results.
|Item Type:||Article (Refereed Research - C1)|
|Keywords:||natural convection; ramp cooling; boundary layer; unsteady flow; instability|
|FoR Codes:||09 ENGINEERING > 0915 Interdisciplinary Engineering > 091504 Fluidisation and Fluid Mechanics @ 100%|
|SEO Codes:||97 EXPANDING KNOWLEDGE > 970109 Expanding Knowledge in Engineering @ 100%|
|Deposited On:||15 Apr 2011 15:57|
|Last Modified:||05 May 2013 01:32|
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|Citation Counts with External Providers:||Web of Science: 6|
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